Image3_Internal structure and water routing of an ice-debris landform assemblage using multiple geophysical methods in the semiarid Andes.JPEG

• Main Authors: Gonzalo Navarro, Rémi Valois, Shelley MacDonell, Giulia de Pasquale, Juan Pablo Díaz
• Format: Still Image
• Language: unknown
• Published: 2023
• Subjects: Solid Earth Sciences; Climate Science; Atmospheric Sciences not elsewhere classified; Exploration Geochemistry; Inorganic Geochemistry; Isotope Geochemistry; Organic Geochemistry; Geochemistry not elsewhere classified; Igneous and Metamorphic Petrology; Ore Deposit Petrology; Palaeontology (incl. Palynology); Structural Geology; Tectonics; Volcanology; Geology not elsewhere classified; Seismology and Seismic Exploration; Glaciology; Hydrogeology; Natural Hazards; Quaternary Environments; Earth Sciences not elsewhere classified; Evolutionary Impacts of Climate Change; applied geophysics; cryosphere; debris-covered glacier; mountain hydrology; rock glacier; water transfers; Glacier Mountain; Ice; permafrost
• Online Access: https://doi.org/10.3389/feart.2023.1102620.s003; https://figshare.com/articles/figure/Image3_Internal_structure_and_water_routing_of_an_ice-debris_landform_assemblage_using_multiple_geophysical_methods_in_the_semiarid_Andes_JPEG/22648546

Rock glaciers are the most abundant (peri) glacial landform in the semiarid Andes (SA, 29–34°S), covering about three times the area of mountain glaciers. Recent studies suggest they may play an important hydrological role, including generating, storing and routing water. However, processes governin...